Dugway Range

With the elevation of the Great Salt Lake about 4,200 ft (1,280 m) (4,196 ft (1,279 m), in 2006), and Bonneville Salt Flats, at 4,219 ft (1,286 m), the surrounding salt flats around the mountain range, are about 4,220 ft (1,286 m). Between the Fish Lakes to the southwest, actual foothills above the Great Salt Lake Desert saltflats exist. Washes converge off the southwest flank; they flow southwest, then converge in a shallow valley, with three washes flowing northwest to the GSLD saltflat. Adjacent southwest is a circular, Black Rock Hills, 5,554 feet (1,693 m), (1,334 ft (407 m) prominence, 5 mi (8 km) diameter), 4 mi (6 km) east of the Fish Lakes, and about 8 mi (13 km) due southwest of the Dugway foothills.

Northeast of the Dugway Range, and east of Granite Mountain are the GSLD salt flats. They extend halfway southeast, along the range's northeast flank, to meet the outflow terminus at the northwest of Dugway Valley, which itself trends mostly southeast, about 17 mi (27 km). The valley contains Table Mountain Reservoir (0.15 mi (0 km) diameter), located 3 mi (5 km) due-west of Table Mountain, 5,766 ft (1,757 m). Dissected hills and flats border the valley's northeast; also, with the same northwest trendline as the Dugways, the Old River Bed courses along, about 15 mi (24 km), a circuitous wash-bed, containing Old River Bed Road.

South of the range at Pony Express Road, is Dugway Pass. The Dugway foothills from here merge south and south-southeast into the northern foothills of the Thomas Range.

Adjacent at the south terminus of Granite Mountain, is a small rock "island", Sapphire Mountain, 4,791 ft (1,460 m), 1.5 mi (2 km) long (571 ft (174 m) prominence). Sapphire Mountain is 2.55 mi (4 km) from the Dugway foothills, and 0.5 mi (1 km) from the Granite Mountain perimeter.